A photograph of people examining a section of road lying on the Greendale Fault line which has large cracks caused by the 4 September 2010 earthquake. Police tape and cones have been used to close off the road.
A photograph of a fence on the Greendale Fault line which has shifted considerably due to the 4 September 2010 earthquake. Police tape and cones have been placed across the road to close it off.
A photograph of people examining a section of road lying on the Greendale Fault line which has large cracks caused by the 4 September 2010 earthquake. Police tape and cones have been used to close off the road.
A photograph of a section of road lying on the Greendale Fault line which has shifted considerably and cracked due to the 4 September 2010 earthquake. In the distance, police tape and cones have been used to close off the road.
A photograph of cracks across a road in Canterbury caused by the 4 September 2010 earthquake.
Telegraph Road was a straight road before the recent 7.1 magnitude earthquake. The fault ran right through here and now the road has a dramatic kink in it.
A photograph of a crack in a field indicating the Greendale faultline. A mobile phone has been placed beside the crack as a size reference.
A photograph of a crack in a field indicating the Greendale faultline. A mobile phone has been placed beside the crack as a size reference.
A photograph of volunteers from the Wellington Emergency Management Office taking photographs of the lateral shifting and cracks in a road after the 4 September 2010 earthquake.
A photograph of a paddock on the Greendale fault line.
A photograph of a paddock on the Greendale fault line.
We present ground motion simulations of the Porters Pass (PP) fault in the Canterbury region of New Zealand; a major active source near Christchurch city. The active segment of the PP fault has an inferred length of 82 km and a mostly strike-slip sense of movement. The PP fault slip makes up approximately 10% of the total 37 mm/yr margin-parallel plate motion and also comprises a significant proportion of the total strain budget in regional tectonics. Given that the closest segment of the fault is less than 45 km from Christchurch city, the PP fault is crucial for accurate earthquake hazard assessment for this major population centre. We have employed the hybrid simulation methodology of Graves and Pitarka (2010, 2015), which combines low (f<1 Hz) and high (f>1 Hz) frequencies into a broadband spectrum. We have used validations from three moderate magnitude events (𝑀𝑤4.6 Sept 04, 2010; 𝑀𝑤4.6 Nov 06, 2010; 𝑀𝑤4.9 Apr 29, 2011) to build confidence for the 𝑀𝑤 > 7 PP simulations. Thus far, our simulations include multiple rupture scenarios which test the impacts of hypocentre location and the finite-fault stochastic rupture representation of the source itself. In particular, we have identified the need to use location-specific 1D 𝑉𝑠/𝑉𝑝 models for the high frequency part of the simulations to better match observations.
A report by Thomas Wilson, Zach Whitman, Matt Cockcroft, Mike Finnemore, Peter Almond, Derrick Moot, et al on various remediation techniques for farms on the Greendale fault scarp. The purpose of the report was to brief the Rural Recovery Group on 20 September 2010.
A photograph of a crack in a paddock on the Greendale fault line.
A photograph of soil uplift in a paddock on the Greendale fault line.
A photograph of a crack in a paddock on the Greendale fault line.
A photograph of soil uplift in a paddock on the Greendale fault line.
A photograph of fault ruptures through a tree plantation on Telegraph Road in Darfield.
A photograph of fault ruptures through a tree plantation on Telegraph Road in Darfield.
A photograph of fault ruptures through a tree plantation on Telegraph Road in Darfield.
A photograph of damage to the ground of a paddock on the Greendale fault line.
A photograph of University of Canterbury Geology students surveying land on the Greendale fault line.
A photograph of damage to the ground of a paddock on the Greendale fault line.
A photograph of damage to the ground of a paddock on the Greendale fault line.
A photograph of damage to the ground of a paddock on the Greendale fault line.
A report by Thomas Wilson, Peter Almond, Derrick Moot, Zach Whitman, Rose Turnbull, et al summarising a reconnaissance survey of farms on the Greendale fault. The purpose of the report was to inform farm and societal recovery. It was presented at a Rural Recovery Group meeting on 13 September 2010.
A photograph of a close up view of a fault rupture through a tree plantation on Telegraph Road in Darfield.
A photograph of the Greendale Fault line, now visible across a paddock due to cracks caused by the 4 September 2010 earthquake.
A photograph of University of Canterbury Geology staff and students using ground penetrating radar (GPR) to survey land on the Greendale fault line.
A photograph of University of Canterbury Geology student Matt Cockcroft using ground penetrating radar (GPR) to survey land on the Greendale fault line.